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<![CDATA[PENURUNAN PERMUKAAN AIR DANAU ANEUK LAOT DI PULAU WEH PROPINSI NANGROE ACEH DARUSSALAM ]]>
<![CDATA[Edyanto, CB Herman]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
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<![CDATA[One of the main duties of the Local Government of Sabang was the preparation of fresh water for the people which is supplied from the lake of Aneuk Laot in WehIsland. The problem concerning with this lake is that the water level become decreasing significantly. Earthquake in a big scale which was occured in the year of 2004 was pointed at the causal factor to enlarge breaking residing in lake base. To find the answer of it, therefore, should be met.]]>
<![CDATA[PEAT CARBON, CIRE AND CLIMATE INTERACTIONS ]]>
<![CDATA[Aldrian, Edvin]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
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<![CDATA[This study describes the interaction between forest fire and climate, which focuses on the peatland fire contribution and its carbon released. We established the interannual carbon released that refer to some previous result and we extend the results for the last decade(1997 to 2007) of total carbon and PM10 estimations. We found a significant relationship betweenclimate and hotspot number, which indicate the behavior of fires over Sumatera and Kalimantan over the last decade, except for 2006. Improvement in the correlation occurs when we utilized second half of the year in to consideration. Apparently there are two regional climatic systemsthat drive or force the annual variability of hotspots over Sumatera and Kalimantan through trans equatorial cold surge in the first half of year and El Nino in the second half of the year. The cold surge phenomenon is crucial for the hotspot variability for Riau province, while the latter could impacts both Sumatera and Kalimantan. Strong climate forcing indicates, by excluding 2006, that Indonesian peat pool is vulnerable to the regional climatic system or a victim of regional climate perturbation. Recent data (latest four years) shows larger fluctuation from the climatic factor. The 2006 fires and their emission are exceptionally high and divert from the strong correlation between fire and climatic factor. The 2006 fire close to 1997 firein amount and emission (88.4%) and PM10 (87%) and hotspot number (92.8%). Overall, during the last decade, the carbon emission from forest fires in Indonesia fluctuates following climate variability and could not be generalized to emit carbon at persistently high level every year.]]>
<![CDATA[PENGARUH IRIGASI DAN NAUNGAN TERHADAP PRODUKSI TANAMAN CABE (CAPSICUM ANNUM) PADA LAHAN BERPASIR DI PANTAI GLAGAH, YOGYAKARTA ]]>
<![CDATA[Mawardi, Ikhwanuddin]]>;
<![CDATA[Sudaryono, Sudaryono]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
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<![CDATA[Coastal area is one of the marginal areas that is not suitable for agriculture field. However, bad quality of the area can be improved physically and chemically by adding some organic matters into the soil. Another factor that also plays an important role in improving the quality of sandy soil is weather, which consists of sun radiation, temperature, humidity, soil temperature, wind flow and rain fall. In order to obtain a good quality micro weather in a chili vegetation field, a cover may be placed above the vegetation to create a warm and wet micro weather which will free the vegetation from stress. Another important thing to attain success in productive agriculture is a certainty to get water or irrigation that can be engineered. Through those environmental engineering, an improvement on chili harvesting product has been achieved at Glagah Coast, West Progo, Yogyakarta.]]>
<![CDATA[ASPEK GEOHIDROLOGI DALAM PENENTUAN LOKASI TAPAK TEMPAT PEMBUANGAN AKHIR SAMPAH (TPA) ]]>
<![CDATA[Wibowo, Mardi]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
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<![CDATA[Final Waste Disposal Facilities (FWDF) often pollute the environment,especially in city that have limited area. Groundwater pollution is one of negative impact that is caused FWDF. For minimized the environmental pollution, FWDF should located at area that geologically appropriate. Regional feasibility analysis for FWDF especially from geohydrological aspect is the best first selection step for determine location of FWDF. Geohydrologival aspect include lithology, groundwater water table, slope, rainfall intensity, distance to river, distance to shoreline, distance to fault, volcano eruption, flood and conservation zone.]]>
<![CDATA[CAD_TOOL (CAGE AQUACULTURE DECISION SUPPORT TOOL) PERANGKAT PENDUKUNG KEPUTUSAN DALAM BUDIDAYA KERAMBA JARING APUNG ]]>
<![CDATA[Santoso, Arif Dwi]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
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<![CDATA[CADS_TOOL is a software decision support tool for floating net cages management which constructs of two elemens, software and technic module. It has been developed by the copyright holders (the Australian Centre of International Agriculture Research (“ACIAR”), the Australian Institute of Marine Science (“AIMS”) and the Departemen Kelautan dan Perikanan (“DKP” : Ministry of Marine Affairs and Fisheries, Indonesia)as a tool. The objective of this software is to classify a site, to select the best site from several site alternatives, to calculate the sustainable holding density of a chosen site and to perform a basic economic appraisal of a farm at that site. CADS_TOOL includes 4 models for calculating holding or carrying capacity as sub-tabs under the Holding Capacity tab. For marine cages, the methods used are: Simplified MOM based on Stigebrandt et al., (2004), Tookwinas et al. (2004) and Hanafi et al. (2006), while Pulatsü et al. (2003) is used for freshwater cages in lakes/dams. In this paper will describe only a Tookwinas model.]]>
<![CDATA[PENURUNAN PERMUKAAN AIR DANAU ANEUK LAOT DI PULAU WEH PROPINSI NANGROE ACEH DARUSSALAM ]]>
<![CDATA[Edyanto, CB Herman]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
Show Abstract
|
Download Original
|
Original Source
|
Check in Google Scholar
|
Full PDF (121.052 KB)
<![CDATA[One of the main duties of the Local Government of Sabang was the preparation of fresh water for the people which is supplied from the lake of Aneuk Laot in WehIsland. The problem concerning with this lake is that the water level become decreasing significantly. Earthquake in a big scale which was occured in the year of 2004 was pointed at the causal factor to enlarge breaking residing in lake base. To find the answer of it, therefore, should be met.]]>
<![CDATA[PEAT CARBON, CIRE AND CLIMATE INTERACTIONS ]]>
<![CDATA[Aldrian, Edvin]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
Show Abstract
|
Download Original
|
Original Source
|
Check in Google Scholar
|
Full PDF (112.447 KB)
<![CDATA[This study describes the interaction between forest fire and climate, which focuses on the peatland fire contribution and its carbon released. We established the interannual carbon released that refer to some previous result and we extend the results for the last decade(1997 to 2007) of total carbon and PM10 estimations. We found a significant relationship betweenclimate and hotspot number, which indicate the behavior of fires over Sumatera and Kalimantan over the last decade, except for 2006. Improvement in the correlation occurs when we utilized second half of the year in to consideration. Apparently there are two regional climatic systemsthat drive or force the annual variability of hotspots over Sumatera and Kalimantan through trans equatorial cold surge in the first half of year and El Nino in the second half of the year. The cold surge phenomenon is crucial for the hotspot variability for Riau province, while the latter could impacts both Sumatera and Kalimantan. Strong climate forcing indicates, by excluding 2006, that Indonesian peat pool is vulnerable to the regional climatic system or a victim of regional climate perturbation. Recent data (latest four years) shows larger fluctuation from the climatic factor. The 2006 fires and their emission are exceptionally high and divert from the strong correlation between fire and climatic factor. The 2006 fire close to 1997 firein amount and emission (88.4%) and PM10 (87%) and hotspot number (92.8%). Overall, during the last decade, the carbon emission from forest fires in Indonesia fluctuates following climate variability and could not be generalized to emit carbon at persistently high level every year.]]>
<![CDATA[PENGARUH IRIGASI DAN NAUNGAN TERHADAP PRODUKSI TANAMAN CABE (CAPSICUM ANNUM) PADA LAHAN BERPASIR DI PANTAI GLAGAH, YOGYAKARTA ]]>
<![CDATA[Mawardi, Ikhwanuddin]]>;
<![CDATA[Sudaryono, Sudaryono]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
Show Abstract
|
Download Original
|
Original Source
|
Check in Google Scholar
|
Full PDF (55.032 KB)
<![CDATA[Coastal area is one of the marginal areas that is not suitable for agriculture field. However, bad quality of the area can be improved physically and chemically by adding some organic matters into the soil. Another factor that also plays an important role in improving the quality of sandy soil is weather, which consists of sun radiation, temperature, humidity, soil temperature, wind flow and rain fall. In order to obtain a good quality micro weather in a chili vegetation field, a cover may be placed above the vegetation to create a warm and wet micro weather which will free the vegetation from stress. Another important thing to attain success in productive agriculture is a certainty to get water or irrigation that can be engineered. Through those environmental engineering, an improvement on chili harvesting product has been achieved at Glagah Coast, West Progo, Yogyakarta.]]>
<![CDATA[ASPEK GEOHIDROLOGI DALAM PENENTUAN LOKASI TAPAK TEMPAT PEMBUANGAN AKHIR SAMPAH (TPA) ]]>
<![CDATA[Wibowo, Mardi]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
Show Abstract
|
Download Original
|
Original Source
|
Check in Google Scholar
|
Full PDF (23.164 KB)
<![CDATA[Final Waste Disposal Facilities (FWDF) often pollute the environment,especially in city that have limited area. Groundwater pollution is one of negative impact that is caused FWDF. For minimized the environmental pollution, FWDF should located at area that geologically appropriate. Regional feasibility analysis for FWDF especially from geohydrological aspect is the best first selection step for determine location of FWDF. Geohydrologival aspect include lithology, groundwater water table, slope, rainfall intensity, distance to river, distance to shoreline, distance to fault, volcano eruption, flood and conservation zone.]]>
<![CDATA[CAD_TOOL (CAGE AQUACULTURE DECISION SUPPORT TOOL) PERANGKAT PENDUKUNG KEPUTUSAN DALAM BUDIDAYA KERAMBA JARING APUNG ]]>
<![CDATA[Santoso, Arif Dwi]]>
<![CDATA[ Jurnal Hidrosfir Indonesia Vol 3, No 1 (2008) ]]>
Publisher : <![CDATA[Jurnal Hidrosfir Indonesia ]]>
Show Abstract
|
Download Original
|
Original Source
|
Check in Google Scholar
|
Full PDF (80.38 KB)
<![CDATA[CADS_TOOL is a software decision support tool for floating net cages management which constructs of two elemens, software and technic module. It has been developed by the copyright holders (the Australian Centre of International Agriculture Research ( ACIAR ), the Australian Institute of Marine Science ( AIMS ) and the Departemen Kelautan dan Perikanan ( DKP : Ministry of Marine Affairs and Fisheries, Indonesia)as a tool. The objective of this software is to classify a site, to select the best site from several site alternatives, to calculate the sustainable holding density of a chosen site and to perform a basic economic appraisal of a farm at that site. CADS_TOOL includes 4 models for calculating holding or carrying capacity as sub-tabs under the Holding Capacity tab. For marine cages, the methods used are: Simplified MOM based on Stigebrandt et al., (2004), Tookwinas et al. (2004) and Hanafi et al. (2006), while Pulats et al. (2003) is used for freshwater cages in lakes/dams. In this paper will describe only a Tookwinas model.]]>
